Meandering streamflows across landscapes and scales: a review and discussion

This introductory chapter reviews the history of research on meandering streams and presents a compilation of data on meander morphology.

July 11, 2024 · A. Finotello, P. R. Durkin, Z. Sylvester

Turbidite correlation for paleoseismology

Marine turbidite paleoseismology relies on the assumption of synchronous triggering of turbidity currents by earthquake shaking to infer rupture extent and recurrence. Such inference commonly depends …

June 18, 2024 · N. M. Nieminski, Z. Sylvester, J. A. Covault, J. Gomberg, L. Staisch, I. W. McBrearty

Fluvial-style migration controls autogenic aggradation in submarine channels: Joshua Channel, eastern Gulf of Mexico

There has been debate over the processes acting on deep-water channels, with comparisons made to the evolution of meandering fluvial systems. We characterized a three-dimensional seismic-reflection da…

June 1, 2024 · P. D. Morris, Z. Sylvester, J. A. Covault, D. Mohrig, D. Dunlap

The impact of post-cutoff bend curvature on channel kinematics in meandering rivers: an example from the Trinity River, Texas, USA

This paper investigates the relationship between post-cutoff bend curvature and channel kinematics in meandering rivers using Trinity River data.

June 1, 2024 · C. M. Speed, Z. Sylvester, P. D. Morris, D. Mohrig

Stratigraphy in space and time: A reproducible approach to analysis and visualization

Time-elevation plots and chronostratigraphic diagrams are valuable for understanding and analyzing stratigraphy when time-elevation data, or some approximation of them, are available, for example in f…

February 5, 2024 · Z. Sylvester, K. M. Straub, J. A. Covault

Automated multi-well stratigraphic correlation and model building using relative geologic time

Stratigraphic correlation of geophysical well logs is one of the most importantand most time-consuming—tasks that applied geoscientists perform on a daily basis. Using the dynamic time warping (DTW) a…

May 23, 2023 · Z. Sylvester